概括
微量元素的图案揭示了互补的玄武岩来源,表明地幔分化和岩海洋进化. 这项研究估计了源区域的大小及其地幔分布.
科学领域:
- 地质化学 地质化学
- 石化学 石化学是一门学科.
- 地幔动力学地幔动力学
背景情况:
- 大陆,海洋岛屿和中洋山脊玄武岩表现出不同的微量元素模式.
- 了解这些模式是解读地幔组成和演变的关键.
研究的目的:
- 用微量元素数据估计基岩源区域的相对大小.
- 阐明创造了独特的地幔储库的分化过程.
主要方法:
- 对各种玄武岩类型的微量元素度模式的分析.
- 斗源区域体积和组成的建模.
主要成果:
- 互补的微量元素图案表明不同的,分离的地幔源区域.
- 这些来源的综合体积占据了上层地幔的大部分.
- 中洋山脊玄武岩来源是从生态石积聚物进化而来的,而其他来源则是丰富的石榴.
结论:
- 早期的地幔分化和晶体分化导致了玄武岩源区域的分离.
- 这些发现支持地幔异质性的陆地岩海洋起源模型.
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